Where: Isfahan, Iran (33.1° N, 52.0° E: paleocoordinates 29.4° N, 40.0° E)
• coordinate stated in text
• small collection-level geographic resolution
When: Nayband Formation, Norian (228.0 - 208.5 Ma)
• the Triassic deposits are overlain with a distinct angular unconformity by the Lower Cretaceous deposits, whereas Jurassic sediments are missing almost completely. The unit of conglomerate at the base of the Lower Cretaceous contains pebbles of carbonate and siliciclastic rocks without any sign of the Jurassic fossils.
• member-level stratigraphic resolution
Environment/lithology: reef, buildup or bioherm; lithified limestone
Size classes: macrofossils, mesofossils
Primary reference: M. Mannani and M. Yazdi. 2009. Late Triassic and Early Cretaceous sedimentary sequences of the northern Isfahan Province (Central Iran): stratigraphy and paleoenvironments. Boletín de la Sociedad Geológica Mexicana 61(3):367-374 [W. Kiessling/M. Krause]more details
Purpose of describing collection: general faunal/floral analysis
PaleoDB collection 138967: authorized by Wolfgang Kiessling, entered by Mihaela Krause on 05.02.2013
Creative Commons license: CC BY (attribution)
Taxonomic list
unclassified | |
Anthozoa | |
Crassistella juvavica Frech 1890 stony coral | |
Distichomeandra austriaca Frech 1890 stony coral | |
Distichophyllia cf. norica, Oedalmia norica, Cuifia gigantella, Cuifia columnaris, Retiophyllia norica
Distichophyllia cf. norica Frech 1890 stony coral
Oedalmia norica Frech 1890 stony coral
Cuifia gigantella stony coral
Cuifia columnaris Roniewicz 1995 stony coral
Retiophyllia norica Frech 1890 stony coral | |
Gastropoda | |
Cryptaulax inaequelineata Nützel and Senowbari-Daryan 1999 snail | |
Purpuroidea dilophosignata periwinkle | |